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Hydrology, Erosion, and Sedimentation

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Hydrology".

Deadline for manuscript submissions: closed (20 December 2023) | Viewed by 1024

Special Issue Editor


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Guest Editor
Institute of Geology and Petroleum Technologies, Kazan (Volga Region) Federal University, Kazan, Russia
Interests: geomorphology; erosion; sediment; sediment flux; river; river basin; climate change; land-use changes; small catchments

Special Issue Information

Dear Colleagues,

The processes of erosion and sedimentation reflect the interaction of two components of the environment—surface runoff and underlying rocks of the lithosphere. At the same time, all water flows within their catchments, from slope watercourses caused by rains or snowmelt to river mouths, form single fluvial systems with their own unique features, depending on a set of environmental and anthropogenic factors, controlling these processes. The study of erosion and sedimentation in their interrelationship and interdependence allows a deeper understanding of the patterns of functioning and development of catchment geosystems of different scales and environments and, consequently, the use of the most optimal strategies for managing these geosystems.

Contributions on the following and related topics are welcome:

  • Erosion and sedimentation in the upper links of the fluvial network: erosion and sedimentation of temporary non-channel (soil erosion) and channel (gullies, ravines, small dry valleys, etc.) flows;
  • Erosion and sedimentation in riverbeds and floodplains;
  • Erosion and sedimentation in river mouths;
  • Formation, transport, and pollution of sediments in permanent and temporary watercourses on various space/time scales;
  • New approaches and methods in the study of erosion and sedimentation;
  • Climate as a factor of erosion and sedimentation processes: from geological antiquity to the present;
  • Human activity and erosion and sedimentation processes in the Anthropocene: from fieldworks to modeling;
  • Biotic factors of erosion and sedimentation processes.

Dr. Artyom Gusarov
Guest Editor

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Published Papers (1 paper)

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Research

29 pages, 13753 KiB  
Article
Runoff of Water and Its Quality under the Combined Impact of Agricultural Activities and Urban Development in a Small River Basin
by Fedor N. Lisetskii and Zhanna A. Buryak
Water 2023, 15(13), 2443; https://doi.org/10.3390/w15132443 - 2 Jul 2023
Cited by 6 | Viewed by 1776
Abstract
The basin of the small river studied here (the Vezelka River, Belgorod Oblast of European Russia) is located within an urban area (22% of the basin). This circumstance determines its specificity as an object of synergetic anthropogenic impact. The purpose of the work [...] Read more.
The basin of the small river studied here (the Vezelka River, Belgorod Oblast of European Russia) is located within an urban area (22% of the basin). This circumstance determines its specificity as an object of synergetic anthropogenic impact. The purpose of the work was to develop and test approaches to the integral assessment of the hydroecological situation both in the watershed and riparian zones based on hydrological, hydrochemical, and hydrobiological data and estimates of soil erosion, river water quality, and the pollution of river bottom sediments. The selection of the Vezelka River and its watershed for the study was due to the presence there of two water intakes for a town with a population of 2439 people per sq. km, repeated bottom deepening in the riverbed, and the fact that there is a single regional small-river hydrological station (although there are 567 rivers < 25 km long in Belgorod Oblast). Analysis for 1951–2021 showed a steady decline in water discharge since 1991; thus, over the past three decades, the discharge has decreased by 2.4 times. The reduction in the length of the river network of the study region by 38% over the past 250 years and the assignment of water (at 10 gauging stations) to 3–4 quality classes (extremely and heavily polluted) indicated the exhaustion of the possibilities for the self-purification of the river water. These estimates for large and medium rivers were clearly confirmed by the investigation of the water in the small river studied. In the summer low-water periods, the maximum allowable concentrations in fishery water bodies were exceeded by 2–10 times in terms of Cu, Fe, ammonium, oil, and biochemical oxygen demand. The reconstruction of the floodplain–channel subsystem of river–valley landscapes was substantiated as the final stage of the concept of basin nature management, replacing the continuous deepening of the channel without proper erosion control measures in the watershed area and the organization of buffer zones along the river banks. Full article
(This article belongs to the Special Issue Hydrology, Erosion, and Sedimentation)
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